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• W2058882694 abstract "Abstract Reservoir characterization requires accurate estimates of permeability. The commonly used porosity-permeability transforms are often inadequate as permeability is also a function of clay distribution, sorting, pore connectivity, tortuosity and variations in other petrophysical properties. More robust permeability estimation can be made by integrating multiple logs in the transform instead of just porosity. This paper deals with a novel technique for deriving permeability by correlating multiple well logs with core permeability using non-parametric regression methods. First, we classify the well log data into electrofacies based on the 'similarity' of their response. This electrofacies classification does not require any artificial subdivision of the data population but follows naturally based on the unique data values reflecting minerals and lithofacies. A combination of principal component and model-based cluster analysis are used to characterize the electrofacies. Secondly, we apply a non-parametric regression technique to predict permeability using well logs within each electrofacies. The main advantage of this technique is that it is primarily data-driven as opposed to model driven and does not require a priori specification of functional forms, which makes conventional multiple regressions difficult and often biased. The proposed technique was used in a deepwater reservoir system consisting of thick massive sand beds along with thinly bedded sand-shale sequences. The work flow consists of electrofacies identification, facies-wise permeability transform generation, calibration with DST data, and finally permeability population in the geological model using cloud transforms and Sequential Gaussian Simulation (SGS). The permeability transforms generated from core and well log data were validated via blind tests whereby we predicted permeability in another cored well that was not included in the correlation. For further validation, we also used the transform-derived permeabilities in analyzing the DST results in a blind well where a laminated sand section was tested. A reasonable match of the permeability-thickness product was observed. Finally, the permeability transforms were integrated into a 3-D geologic modeling using SGS and cloud transform. It was observed that our approach correctly captured the porosity-permeability scatter in the geologic model for various facies groups. Introduction In this paper an integrated permeability modeling has been carried out for a deepwater channel-levee complex of a gas reservoir. This field is located in Krishna Godavari Basin in the Bay of Bengal, east of India. The Krishna Godavari basin is in the central part of the eastern passive continental margin. The different plays in the reservoir system include channel facies, overbank and levees of Pliocene age. The channel facies consist mostly of thick clean sands while overbank and levee consist of thin laminated sand / shale sequences. Core analysis results are available from three wells in this reservoir. Most of the core plugs are from thick sands. A DST has been carried out in another set of three wells. The DST intervals in these wells comprised of both clean and laminated thin sands. Most of the well log suites are available in all the drilled wells. The porosity-permeability correlation developed earlier for thin laminated sands was based on the DST data and limited core data and was unable to capture the porosity-permeability relationships conclusively. The purpose of this study was to integrate all the available data in a consistent manner so that appropriate permeability correlations can be generated for thick clean sands in the reservoir and also, thin laminated sands which have been particularly challenging to characterize in the past." @default.
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• W2058882694 date "2008-03-04" @default.
• W2058882694 modified "2023-10-18" @default.
• W2058882694 title "Integrated Permeability Modeling Using Wireline Logs, Core and DST Data in a Deepwater Reservoir" @default.
• W2058882694 doi "https://doi.org/10.2118/113599-ms" @default.
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